Title

Authors

Document Type

Article

Publication Date

2-2018

DOI

http://dx.doi.org/10.1016/j.precamres.2017.10.001

Abstract

The Columbia (Nuna) supercontinent existed from approximately 1.9 Ga to 1.3 Ga. Laurentia was part of Columbia, and the western edge of Laurentia (current coordinates) was likely proximal to a large landmass during parts of this interval. Here, we present detrital zircon ages of a Paleoproterozoic sedimentary succession in northern Yukon, Canada, that bear on the evolution of Columbia. The sedimentary succession is preserved as clasts within 1.60 Ga hydrothermal megabreccias. Analyses of detrital zircon reveal abundant 1.78–1.68 Ga zircon with evolved Hf isotope values (−16.1